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File:Bulletin de la Société géologique de France (1893) (14749989756).jpg

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Identifier: bulletindelasoci3211893soci (find matches)
Title: Bulletin de la Société géologique de France
Year: 1830 (1830s)
Authors: Société géologique de France
Subjects: Geology
Publisher: Paris : La Société
Contributing Library: Smithsonian Libraries
Digitizing Sponsor: Smithsonian Libraries

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Text Appearing Before Image:
int 685 de la carte de lEtat-major(confluent) et en se dirigeant vers le sommet du plateau dEycenac,nous trouvons successivement : 1° Des sables à Mastodontes reposant sur lOligocène ; 2° Une coulée de basalte (p° inférieur de la coupe) ; 3° Des sables et cailloux roulés avec phonolite abondant (p°) ; 4° Des tufs et des brèches basaltiques (p p°) ; 5° Une nouvelle coulée basaltique (p) ; 6 Sables à Mastodontes, dépourvus de cailloux roulés (p°) ; 7° Brèches basaltiques (p (3°) identiques à celles de Ceyssac, deDenise, du rocher Corneille ; 50- dépaisseur; 8° Basalte pliocène supérieur ou basalte des plateaux de la chaînedu Velay. Nous sommes ici vers le fond de lancienne vallée pliocène ; lesdépôts qui ont comblé cette vallée atteignent 150^ dépaisseur. Lacoupe (fig. 5), pratiquée suivant une direction oblique par rapport àla direction du cours deau pliocène, résume les faits observés parla Société. 514 M. BOULE. EXCURSION DU 15 SEPTEMBRE 1893
Text Appearing After Image:
M. BOULE. — EXCURSION DU lô SEPTEMBRE 1893 515 Avant de quitter le plateau dEycenac pour retourner au Puy,par Vais, la Société admire le panorama des environs de cette villeet la disposition des plateaux basaltiques qui entourent la vieillecité comme de gigantesques remparts. Les escarpements forméspar les coulées du Pliocène supérieur dessinent des lignes hori-zontales dune altitude moyenne et uniforme de 800 mètres, seraccordant entre elles admirablement. Le croquis (fig. 6) peut donnerune idée de la physionomie très spéciale que les formes du terraindoivent à cette disposition des plateaux basaltiques. Il est évidentque les éruptions du Pliocène supérieur ont fini par niveler complè-tement cet ancien creux du Puy, que les alluvions et les éruptionsdu Pliocène moyen avaient en partie comblé. Cest à travers toutcet ensemble que les eaux ont ensuite creusé les vallées actuelles etsculpté ladmirable paysage que nous avons sous les yeux. COMPTE RENDU DE LEXCUR

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https://www.flickr.com/photos/internetarchivebookimages/14749989756/

Author Société géologique de France
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Volume
InfoField
1893
Flickr tags
InfoField
  • bookid:bulletindelasoci3211893soci
  • bookyear:1830
  • bookdecade:1830
  • bookcentury:1800
  • bookauthor:Soci__t___g__ologique_de_France
  • booksubject:Geology
  • bookpublisher:Paris___La_Soci__t__
  • bookcontributor:Smithsonian_Libraries
  • booksponsor:Smithsonian_Libraries
  • bookleafnumber:673
  • bookcollection:biodiversity
  • bookcollection:americana
  • BHL Collection
  • BHL Consortium
Flickr posted date
InfoField
29 July 2014
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